6,202 Works

Investigation of submarine landforms in Potter Cove, King George Island, Antarctic Peninsula, supplement to: Wölfl, Anne-Cathrin; Wittenberg, Nina; Feldens, Peter; Hass, H Christian; Betzler, Christian; Kuhn, Gerhard (2016): Submarine landforms related to glacier retreat in a shallow Antarctic fjord. Antarctic Science, Antarctic Science, 28(06), 475-486

Anne-Cathrin Wölfl, Nina Wittenberg, Peter Feldens, H Christian Hass, Christian Betzler & Gerhard Kuhn
Since the Last Glacial Maximum, ice has retreated through the fjords of the South Shetland Islands leaving a valuable record of submarine landforms behind. In this study, glacial landforms and sub-bottom characteristics have been mapped to investigate the late Holocene retreat behaviour of the Fourcade Glacier and to delineate past environmental processes in Potter Cove, King George Island. The comprehensive datasets include high-resolution swath bathymetry, shallow seismic profiling and one sediment core. Moraines, moraine incisions...

PARADIGM pathway analysis of mRNASeq expression data

PARADIGM pathway analysis of mRNASeq expression and copy number data

CHASM (Cancer-Specific High-throughput Annotation of Somatic Mutations)

CHASM (Cancer-Specific High-throughput Annotation of Somatic Mutations)

Minerals of bulk and fine-grained (2 µm) samples from DSDP Leg 60, supplement to: Latouche, Claude; Maillet, Noelle; Blanchet, R (1982): X-ray mineralogy studies, Deep Sea Drilling Project Leg 60. In: Hussong, DM; Uyeda, S; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 60, 437-453

Claude Latouche, Noelle Maillet & R Blanchet
A bulk-sediment and clay-fraction X-ray diffraction study of samples from Deep Sea Drilling Project Leg 60 shows an abundance of the following minerals: plagioclase feldspar, zeolite, smectite, Fe-Mg chlorite, attapulgite, and serpentine. Amorphous compounds are also abundant.The variations in abundance of the different components correspond to episodes of volcanic activity through time. Deposits from periods of great activity are composed of sediments very rich in amorphous matter and in "primary" minerals (e.g., plagioclase feldspars). During...

Geochemistry at DSDP Leg 60, supplement to: Desprairies, Alain (1982): Authigenic minerals in volcanogenic sediments cored during Deep Sea Drilling Project Leg 60. In: Hussong, DM; Uyeda, S; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 60, 455-466

Alain Desprairies
Eocene to Pleistocene volcanogenic sediments from the Mariana Trough and the Mariana arc-trench system have been studied by X-ray diffraction, X-ray fluorescence, and atomic absorption, and with a scanning electron microscope with an X-ray-energy-dispersive attachment. The mineralogical composition of the volcaniclastic sediments (tuffs) is the same as that of the other associated sediments (mudstones). Diagenetic alterations are significant and seem to result from two processes. The first (low-temperature alteration) develops with age and depth; it...

Analyses of a Holocene soil/loess sequence in Southern Siberia, supplement to: Kravchinsky, Vadim; Langereis, Cornelis G; Walker, Shawn D; Dlusskiy, Konstantin G; White, Dustin (2013): Discovery of Holocene millennial climate cycles in the Asian continental interior: Has the sun been governing the continental climate? Global and Planetary Change, 110(C), 386-396

Vadim Kravchinsky, Cornelis G Langereis, Shawn D Walker, Konstantin G Dlusskiy & Dustin White
We conducted a high-resolution study of a unique Holocene sequence of wind-blown sediments and buried soils in Southern Siberia, far from marine environment influences. This was accomplished in order to assess the difference between North Atlantic marine and in-land climate variations. Relative wind strength was determined by grain size analyses of different stratigraphic units. Petromagnetic measurements were performed to provide a proxy for the relative extent of pedogenesis. An age model for the sections was...

Mineralogy at DSDP Sites 68-502 and 68-503, supplement to: Schumann, Dieter; Nagel, Ulrich (1982): Leg 68: Shore-based x-ray mineralogy. In: Prell, WL; Gardner, JV; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 68, 397-402

Dieter Schumann & Ulrich Nagel
Eighty-four sediment samples from four holes at Site 502 and 54 samples from three holes at Site 503 were analyzed for mineral content by semiquantitative X-ray diffraction methods. Site 502 is located in the Western Caribbean, whereas Site 503 lies in the Eastern Pacific (probably on the north flank of the Galapagos Spreading Center). Both sites were chosen to yield continuous core sections for investigations of late Neogene and Quaternary biostratigraphy and magnetostratigraphy and to...

Stratigraphy of the Campanian-Maastrichtian boundary in ODP Hole 122-762C, supplement to: Thibault, Nicolas; Husson, Dorothée; Harlou, Rikke; Gardin, Silvia; Galbrun, Bruno; Huret, Emilia; Minoletti, Fabrice (2012): Astronomical calibration of upper Campanian–Maastrichtian carbon isotope events and calcareous plankton biostratigraphy in the Indian Ocean (ODP Hole 762C): Implication for the age of the Campanian–Maastrichtian boundary. Palaeogeography, Palaeoclimatology, Palaeoecology, 337-338, 52-71

Nicolas Thibault, Dorothée Husson, Rikke Harlou, Silvia Gardin, Bruno Galbrun, Emilia Huret & Fabrice Minoletti
An integrated framework of magnetostratigraphy, calcareous microfossil bio-events, cyclostratigraphy and d13C stratigraphy is established for the upper Campanian-Maastrichtian of ODP Hole 762C (Exmouth Plateau, Northwestern Australian margin). Bulk-carbonate d13C events and nannofossil bio-events have been recorded and plotted against magnetostratigraphy, and provided absolute ages using the results of the cyclostratigraphic study and the recent astronomical calibration of the Maastrichtian. Thirteen carbon-isotope events and 40 nannofossil bio-events are recognized and calibrated with cyclostratigraphy, as well as...

Chemical composition of igneous rocks and origin of the sill and pillow-basalt complex at DSDP Site 61-462, supplement to: Tokuyama, Hidekazu; Batiza, Rodey (1981): Chemical composition of igneous rocks and origin of the sill and pillow-basalt complex of Nauru Basin, Southwest Pacific. In: Larson, RL; Schlanger, SO; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 61, 673-687

Hidekazu Tokuyama & Rodey Batiza
The sill and pillow complex cored on Deep Sea Drilling Project Leg 61 (Site 462) is divided into two groups, A and B types, on the basis of chemical composition and volcanostratigraphy. The A-type basalt is characterized by a higher FeO*/MgO ratio and abundant TiO2, whereas the B-type basalt is characterized by a lower FeO*/MgO ratio and scarcity of TiO2. The A type is composed of sills interbedded with hyaloclastic sediments, and the B type...

Correlate_CustomClinical_vs_CopyNumber_Arm

Correlate_CustomClinical_vs_mRNAseq

Clustering of Methylation: consensus NMF

Correlation between mRNAseq expression and clinical features

Correlate_CustomClinical_vs_RPPA

Mutation Analysis (MutSig v1.5)

Clustering of RPPA data: consensus NMF

Correlation between miRseq expression and clinical features

Correlate_CustomClinical_vs_Molecular_Subtypes

Correlate_CustomClinical_vs_RPPA

Correlate_CustomClinical_vs_miRseq

Registration Year

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Affiliations

  • Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • Centro europeo di formazione e ricerca in ingegneria sismica (EUCENTRE)
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